斯洛文尼亚沿海水域水下土壤的选定案例

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摘要

土壤主要在大陆,但也在浅水中,即所谓的水下土壤。水下土壤在水面下形成,主要是在浅水、死水的底部,如沼泽、沼泽、湖泊和浅海。在圣巴塞洛缪,研究了三个水下土壤剖面,对它们进行了详细的研究。记录土壤剖面的地点是随机选择的,目的是在每个地点找到不同类型的植被。研究发现,影响地下水土壤形成的因素基本相同;因此,发生了不同强度的相同成土过程。因此,在每个地点都开发了相同的,非常相似的水下土壤类型。所有的样本都是通过排水管道和挖掘在水下收集的。样品在管道中被排干。在实验室中,根据确定的视界进行目视观察和标准分析。根据WRB分类,将斯洛文尼亚沿海水域的水下土壤分为参考类群Gleysols和arennosols。
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SELECTED CASES OF SUBAQUEOUS SOILS IN SLOVENIAN COASTAL WATERS
Selected cases of subaqueous soils in Slovenian coastal waters The soil is mainly on the mainland, but also in shallow waters, the so-called subaqueous soils. Subaqueous soils form under the water surface, mainly on the bottom of shallow, stagnant waters such as bogs, swamps, lakes, and sea shallows. In St. Bartholomew, three subaqueous soil profiles were studied to investigate them in detail. The sites for recording the soil profiles were selected at random, with the aim of finding a different type of vegetation at each site. We found that the soils were influenced by almost the same factors of subaqueous soil formation; thus, the same soil forming processes of different intensity took place. Therefore, the same, very similar types of subaqueous soils were developed at each site. All samples were collected underwater using drainage pipes and by excavation. The samples were drained in the pipes. In the laboratory, visual observations and standard analysis were performed according to the horizons determined. According to the WRB classification, subaqueous soils in Slovenian coastal waters were classified asreference groups Gleysols and, Arenosols.
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